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多旋回地形
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多旋回地形
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理学
多旋回地形
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polycyclic landform
多旋回地形
在地形发育过程中,由于地壳运动或自然环境的变化,使内、外营力及其作用强度发生多次变化所形成的地形。又称多循环地形、多轮回地形。
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energy dissipation
energy dissipation and damping layer
energy dissipation calculation of hydro-structures
energy dissipation in friction
energy dissipation structure
energy dissipation well
energy dissipator
energy dissipator within tunnel
energy distribution
energy distribution law of microparticles
energy distribution ratio
energy-driven wind
energy economic efficiency
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energy efficiency analysis
energy efficiency labeling
energy efficiency management
energy efficiency of animal house
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energy elasticity index
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energy equation of fluid motion
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